2.1. Linear Response Functions
The probability that probing particles are scattered by a system of interacting adsorbates into a solid angle
, with energy exchange
and parallel momentum transfer
, is the differential reflection coefficient, or cross-section,
. This cross-section is proportional to the DSF,
, according to [
1,
2,
3]
which is directly measured by the HAS technique and gives a measure of the response of the sample through the spontaneous fluctuation spectrum. If, instead, the HeSE technique is used, the response function measured directly is the ISF,
. The two functions are related by a frequency Fourier transform,
The DSF obeys the detailed balance condition [
4,
5,
7]
with
T the surface temperature and
the Boltzmann constant. Equation (
3) states that the probability of a scattering particle losing energy
equals
times the probability of it gaining the same energy at thermal equilibrium.
Within linear response theory [
4,
5,
7], a further important response function is the relaxation function,
, describing the change of a variable after the external perturbation has been switched off. Its Fourier transform,
is related to the DSF as
with
the detailed-balance factor. The relaxation function can also be expressed in terms of the causal, or after-effect, function
,
which is related to the DSF as
This is an alternative expression of the fluctuation-dissipation theorem. The after-effect function is, in general, a real, odd function of time, related to the generalized susceptibility
—whose poles reflect the energy spectrum of the excitations—as
being the Heaviside step function. The susceptibility is complex,
, with even (real) and odd (imaginary/dissipative) parts in
. Equation (
8) can then be written
so that the DSF becomes
It is convenient to introduce, in addition, the retarded Green function associated with
, defined here (following the common convention adopted, e.g., in [
4,
5]) as
Substituting
into Equation (
10) gives the DSF equivalently in terms of the Green function,
From this last expression it is clear that the spectrum of spontaneous fluctuations is related to the dissipative part of the generalized susceptibility (equivalently, of the Green function). Finally, from Equation (
5), an alternative expression to Equation (
4) is
Figure 1 summarizes, schematically, how the ISF and DSF are connected to the other response functions discussed in this Section:
and
are mutually related by the symmetric Fourier transform pair of Equation (
2)—consistent with their both being directly accessible experimentally, by HAS and HeSE, respectively;
in turn determines the causal function
via its inverse Fourier transform, Equation (
24), and determines the dissipative part of the susceptibility,
, via the algebraic inversion of Equation (
10);
and
are, in turn, mutually related by Equation (
6) (a time integral one way, a time derivative the other), and, in the classical limit,
follows directly from
as well; and
follows from
by definition—all linear, invertible operations on the same underlying characteristic function.
2.2. The Characteristic Function Method
Surface diffusion of interacting and non-interacting adsorbates is an open classical/quantum problem, naturally addressed within the theory of stochastic processes: the adsorbates are the system of interest, and the surface (environment) acts as a thermal bath. In the quantum regime, and for not too low surface temperatures, two well-established formalisms are used to obtain the reduced density matrix from the Liouville-von Neumann equation: the Caldeira-Leggett (CL) master equation [
19] and the Lindblad master equation [
20]; in the latter framework, the SWF method has recently been applied [
17,
18,
21]. The ISF can then be written as
where
is the probability (diagonal element of the reduced density matrix) of finding an adsorbate at surface position
at time
t, normalized to unity over the surface. Strictly speaking, Equation (
14) identifies the ISF with the CF of the adsorbate
displacement distribution: the position distribution
coincides with the displacement distribution for the localized initial condition
, assumed throughout. Moreover, since helium scattering is fully coherent, the measured ISF contains, at finite coverage, distinct (pair) correlations in addition to the self part; the single-particle CF reading is exact for the self (tracer) component, and is extended to interacting adsorbates in
Section 2.4 through the effective single-particle ISA model. The second equality shows that the ISF
is the characteristic function (CF) [
24,
25,
27,
28] of the probability distribution of adsorbate positions, with
chosen by the experiment (both its modulus and direction). The CF plays a central role in probability theory as the generating function of moments and cumulants—a fact of particular importance here, since it allows diffusion coefficients to be extracted directly [
22,
23]. We note, in passing, that since only a finite (or at best countable) set of moments is ever accessible experimentally, the question of whether these moments determine the underlying distribution uniquely is, formally, an instance of the classical moment problem [
24]; in the applications discussed below this is not a practical concern, since the CF itself is obtained in closed form, but it is worth keeping in mind when moments alone (rather than the full CF) are used to characterize the diffusion process.
Let the trajectory of an adsorbate lie along surface direction
, so that
, with
K the modulus of the observation direction and
the projection of
along
K as a function of time. If
j vectors
contribute to the total diffusion process,
. Equation (
14) can then be expanded, at
, in terms of moments and cumulants:
with the
n-th moment and cumulant of the jump/transition distribution given by
From Equation (
2), the ISF can also be expanded in the frequency moments (sum rules) of
via a Taylor expansion around
,
with
Interestingly, through Equation (
14) the frequency sum rules depend on the direction of observation and on the surface structure, as well as on thermodynamic and dynamical quantities entering the moments of
—classically, for instance,
. If
is an even function of frequency, only even frequency moments survive.
It should also be noted that the ISF at
is precisely the static structure factor (SSF),
itself a characteristic function of the separation-distance distribution among adsorbates. Following Frenken and Hinch [
29], a simple expression for an adatom overlayer reads
where the 2D lattice vector
runs over the adatom lattice and
is the probability of finding an occupied site at
. Following the same procedure as for the ISF,
with moments and cumulants
These moments and cumulants are essential to characterize the adsorbate distribution and its separation statistics on the surface; from experiment, the SSF is readily extracted as a function of K.
2.4. The Diffusive/Classical Regime
An important simplification is reached at asymptotic times—the diffusive regime, corresponding to times much greater than the inverse of the friction coefficient. In this regime any quantum feature or vestige of the underlying dynamics is lost; diffusion becomes exclusively classical. We have recently analyzed this quantum-to-classical transition explicitly [
26]. Moreover, the asymptotic behavior of the ISF derived below remains valid even in a non-Markovian regime.
In HeSE, the experimental ISF is very precisely fitted to an exponential function of time [
9],
with
constants and
the decaying or dephasing rate. At
, Equation (
34) is constrained by the static structure factor, Equation (
20):
, a useful consistency check on experimental fits. From the inverse Fourier transform of Equation (
2), the DSF (quasi-elastic peak around
) is a Lorentzian,
This rate is an implicit function of the friction coefficient, surface structure, and temperature. The ISF is thus a central dynamical quantity linking diffusion dynamics, structural correlations, and scattering observables.
In the classical limit [
4,
7], i.e., for
so that
, the after-effect function reduces to the classical fluctuation-dissipation form
Substituting Equation (
36) into the definition of the relaxation function, Equation (
6), gives the
exact classical relation between
and
,
Using the exponential form of the ISF, Equation (
34),
, so that
Equation (
37) shows that
and
coincide, up to the constant factor
, only once the asymptotic offset
C has been subtracted; the frequently used shorthand identification
(and, correspondingly,
in frequency space) is therefore exact whenever
— i.e., whenever the ISF fully decays to zero at long times, as is the case for a single mobile adsorbate undergoing unbounded diffusive motion, but not in the presence of a non-decaying (e.g., partly localized or elastic) component of the scattered signal, for which
and the additive shift in Equation (
37) must be kept explicitly. In what follows we adopt
, consistent with the tracer- and collective-diffusion regimes considered in
Section 2.4 and
Section 3, so that
Interestingly, the relaxation function is, in the classical regime, proportional to the time derivative of a characteristic function. From Equations (
34) and (
39), the after-effect function depends exclusively on the dephasing rate and follows the same time behavior as the ISF; as expected,
is an implicit function of surface structure, friction coefficient, and temperature. As shown in
Section 3, it also depends on the jump probabilities and the total jumping rate. Finally, the generalized susceptibility is
whose imaginary (dissipative) part reproduces, via Equation (
10), the Lorentzian DSF of Equation (
35), as it must.
A very general way to obtain the ISF in the diffusive regime exploits the properties of any CF. As anticipated in the Introduction, this route is the CTRW result of Montroll and Weiss [
10,
11] specialized to Poissonian (exponentially distributed) waiting times between jumps; we re-derive it here explicitly, in the CF language, to make its connection to the response-function hierarchy of
Section 2.1,
Section 2.2 and
Section 2.3 transparent. The total displacement of an adsorbate at time
t can be written
with
two-dimensional jump vectors and
the number of jumps up to time
t. Substituting into Equation (
14),
and, since individual jumps are statistically independent and identically distributed for a given number
N of jumps,
i.e., the ISF conditioned on
N jumps,
, is a product of
N identical single-jump CFs. If each jump vector carries probability
,
formally analogous to Equation (
21) for the SSF. If the number of jumps up to time
t,
, follows a Poisson distribution with rate
,
In the limit
, the Poissonian distribution is replaced by a Gaussian one. The dephasing rate for a single adsorbate, or at very low surface coverage
(where adsorbate-adsorbate interactions are negligible), is thus given in full generality by
valid for any Bravais lattice and total jumping rate
, and independent of the specific tight-binding assumptions of
Section 3: the only inputs are (i) that waiting times between jumps are exponentially distributed, and (ii) the single-jump CF,
, itself. For inversion-symmetric jump distributions (
),
is real and so is
; for an asymmetric single-jump distribution,
acquires an imaginary part whose physical content is a drift: the real part still controls the quasi-elastic broadening, while the imaginary part shifts the position of the quasi-elastic peak. All lattice realizations considered below satisfy
, so this distinction plays no role there. The Pauli/Chudley-Elliott result of
Section 3 is recovered as the particular case in which
is evaluated for a simple Bravais lattice (cf. Equation (
21)); any other choice of single-jump distribution—e.g. continuous, non-lattice, or with a different symmetry—yields the same exponential time dependence via Equation (
46), but a different, in general non-periodic,
-dependence of
.
This generalization extends naturally to finite coverage, via the interacting single adsorbate (ISA) model [
14,
15,
16]. The basic idea is to consider two independent noise sources: a Gaussian one, due to the surface acting as a thermal bath (surface friction), and a Poissonian one, due to adsorbate-adsorbate interaction (interpreted as a collisional friction). The adsorbate displacement is thus subject to two independent stochastic processes. At long times, the diffusion process at finite (moderate) coverage reduces to a purely statistical problem, avoiding the need for a specific interaction potential. In the ISA model, the collisional friction is related to
and temperature as [
15]
with
a the unit-cell length along the diffusion direction and
an effective radius of the adsorbate of mass
m. The total displacement at time
t (adsorbates are assumed to remain on surface sites, not on arbitrary lattice points) is now
with
the number of collisions up to time
t. Since a CF factorizes over independent stochastic processes,
Following the same procedure, the Poisson distribution for collisions is identical to Equation (
45) with
and
, so that Equation (
46) becomes
with dephasing rate
As expected, coverage manifests itself as a broadening of the quasi-elastic peak, via Equation (
35) [
16].
A simple and instructive way to characterize the nature of the adsorbate-adsorbate interaction follows from the ratio of the diffusion coefficient at coverage
to that of a single adsorbate. Denoting by
the single-adsorbate friction coefficient—distinct from the total jumping rate
, and related to it through the Einstein relation
—this ratio reads
inversely proportional to the friction coefficients (Einstein relation), times the probability that a neighboring site is free,
, the blocking factor. Equivalently,
—interpretable as the probability that a jump fails because the target site is occupied—is
with
a collisional factor. Once the dephasing rate (or the ISF) is extracted from experiment, the
f-function can be smaller than, equal to, or larger than the coverage, indicating attractive interactions (island formation, increasing the number of available jump sites), the ideal (Langmuir) case, or repulsive interactions (decreasing the number of available sites), respectively. The after-effect function and generalized susceptibility follow, as before, from Equations (
39) and (
40), with
now given by the coverage-dependent expression of Equation (
52).